Julia A. McIntosh
Roger M.H. Smith
Christian A. Sidor
C. Henrik Woolley
2026
<p><span id="_mce_caret" data-mce-bogus="1" data-mce-type="format-caret"><span>The Fremouw Formation of the Central Transantarctic Mountains preserves the southernmost record of Early to Middle Triassic terrestrial ecosystems that developed in the aftermath of the end-Permian mass extinction. Although the well-studied vertebrate fossil assemblage in the lower member of the Fremouw Formation provides a detailed snapshot of subpolar ecosystems immediately following the end-Permian mass extinction, the nature of how long these earliest Triassic communities persisted at the southern extremes of Pangaea is virtually unknown. Importantly, the timing and extent of the major faunal turnover between the lower and upper members of the Fremouw Formation have been obscured by the paucity of fossil specimens historically recovered from the middle member. Here, we describe the first vertebrate assemblage from the middle member of the Fremouw Formation, including occurrences of procolophonids (including </span><span class="italic">Procolophon trigoniceps</span><span>) and archosauromorphs (including </span><span class="italic">Prolacerta broomi</span><span>), as well as infilled vertebrate burrow casts referrable to the ichnogenus </span><span class="italic">Reniformichnus</span><span>. We also summarize and expand on lithostratigraphic shifts between the lower, middle and upper members of the Fremouw Formation. Although the sample size of vertebrate body fossils is small compared to the lower and upper members of the Fremouw Formation, we discuss the evidence for a taphonomic shift between the lower and middle members of the Fremouw Formation that favours preservation of smaller-bodied taxa and individuals in the latter. Together, these preliminary data add crucial context to the persistence of subpolar vertebrate communities in the earliest Mesozoic.</span></span></p>
application/pdf
10.1017/S0954102026100613
en
Cambridge University Press
First vertebrate assemblage from the middle member of the Fremouw Formation (Lower Triassic) of Antarctica
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